SCIENTIFIC ABSTRACT LOMIZE, B.M. - LOMIZE, M.G.

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SCIENTIFIC ABSTRACT
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#7 LOMVE, B. M. 32482. Nekotoryye voprosy proyektirovanlya besplotinnfkh vodozaborov samotectiflogo tipa. Izvestlya Gruz. natich.-issled. in-ta g1drotekhniki I mell-)ratsil, t. 1, 1949, S. 139-48.--.,Iezyujne na gruz. yaz. 50; Letopis' Zhurnallnykh Statey, Vol. 50, Moskva, 11?49 LONIZE, B.H., Inshener. .1 ........I...,......... Locating the dangerous sliding area in calculating the stability of embankments. (VAdr.stroi. 23 no.2:32-36 #54. (KIRA 7:4) (Isibankments) LOMIMP G.M., doktor tekhn.nauk., prof.; ZIAILIROV, R.S.., kand.tekhn.naak Using electroacoustic piezodynamometers in the construction cxf the PlarinwHydroelectric Power Station. Gidr.stroi, 32 no-4:33-35 Ap 162. (MIRA 15 -.4) (Plavinas Hydroelectric Power Station) (Dynamometer) I"IZZ, G. M. ,.; -I , Percolation throu& Crainy C-owAs [with smu&rv in Znglish]. IST. AN Arx.M.Ist.nauki no.1:63-96 146. (XLRA 9: 8) 1. Institut geologichaskiky n&-,tk kkad,%21i nauk Aroyanskor SSR. (Water, Underground) (3oil percolation) LOOMMIZE, 0. M. 32483. Treshchinavataya gornaya poroia, kak srela, so-iarzhashcha-ya fiiltratsionnyy potok. Izvestlyn Gruz. naich.-issled. in-ta gn,irotekhniki i meloratall, t. 1, 1949, 1. 5-12--Rezyume na nz,-Bibitogr: 25 nazv 3~: 1- 1:0. jskv LAW "I Iv 1:4 4.1 "I A, WME, G. M. Filtration In -s. '':,shva, "t, v. ~51 34485) TC17l.U- LOMIZY., T-3ROP 0. M. USSR/Hydrojogy - Irrigation Sep 51 "Counter Filtration Measures in Caaals and Reser- voirs," Prof 0. Jj. Lomize, Prof A. 9. Voznesen- skiy, S. G. KWebaikov, Cand Tech cl "Gidrotekh i Meliorat" Vol III., No 9., PP 7-18 Filtration losses should be kept at min to raise the efficiency of irrigational systems. Results of investigations by Georgian Sci Res Inst of By- draulic'Eng and Soil Improvement were discussed-An a session of Sc:1L Tech Council and Tech Bur. Ar- tificial binding of soils was adopted. Mech re- inforcement, vidoly applied in road.construction, vas recamended-also against filtration. 191757 USSR/Engineering - Civil - Water Filtratior FD-2920 Card 1/1 Pub. 41-1/17 Author Lomize, G. M. and Nasberg., V. M., Moscow, Tbilisi Title Drainage of pressureless hydraulic tunnels Periodical : Izv. AN SSSR, Otd. Tekh. Nauk 3-15, June 1955 Abstract : Points out tne need for having a full understanding of the principles of hydraulic pressure which is developed on the outer walls of a tunnel, or a main by seepage of subterranean water. Describes the most effective ways to drain off this -water, and thus redl.ce tbe pressure on the tunnel walls. Drawings) tables, graph:3, formulae) Six references, all USSR. Institution Submitted April 5, 1955 SOV/1.2-57-9-18476 Tf anslation from: Rtferativnyy zhurnal, Elektrotekhnika, 1957, Nr 9, p 55 (USSR) AUTHOR: Lornize, 0. M. TITLE: Uplift of Gravity Concrete Damji' (Vzveshilvaniye gravitatsionnykh betannykh plotin) PERIODICAL: Tr. Mosk. energ. in-ta, 1956, Nr 19, pp 204-216 ABSTRACT: In conoidering the uplift force and hydrodynam3c pressure exerted by a seeping liquid on the skeleton 6f a percolating medium (concrete, soil), the following assumptions have been made: (1) concrete is considered as a perme- able body; (2) concrete comprises a communicating system of pores; (3) water in concrete pores transmits the hydrostatic pressure that consequently results in an uplift of the skeleton. If a concrete body is dissected by a surface normZ.1 to the seepage path and crossing the minimum quantity of monolithic bridges, the total area of bridges is characterized by an effective -porosity factor n" (F-F, )IF, where F i:3 the total area of crost; -section, F, is the monolithic- bridges area. Experiments show that F, does not exceed 7-9%, whence n, Card 113 SOV/1 1?-57-9-18476 U'plift of Gravity Concrete Dame should be 0.9 or higher; (4) the hyd-rodynarnic pressure of the seepage stream exerted on the solid concrete phase 'is equ&IL to D= -n,, - LV grad h, where Ag is volumetric weight of water, h is the :3-eepage head. As n, is close to 1, the above formula for concrete does not differ much from an exprension for hydrodynamic pressure on the skeleton exerted by a disperse soil: D - - 60 - grad h; (5) loosely bonded water transmits a kydrostatic pressure; (6) the effective-porosity factor can be similarly applied to fissured and porous solid rocks, also subject to uplift; (7) for gravelly and sandy soils (except for cemented) nw - 1; i. e. , these soils do not differ much from concrete as far as uplift and hydrodynamic pressure are concerned; (8) the effect of uplift azd hydrodynamic pressures in clayey soils is not clear, but it can be assumed that nw is close to unity for these soils, too. The effect of water on a structural massif can be determined from the aforesaid. Quantitatively the concrete up- lift in water can be calculated from a simplified formula Auplift r-- Ab - I - If water levels are diff er-ent on both sides of a concrete massif, a seepage Card 2/3 So,,r,, 112-57 -9-18476 Uplift of Gravity Concrete Dams stream (apart from the uplifting pressure) appears and causes a hydrodynamic pressure within the massif. Porosity and seepage peculiarities of corcrete in- fluence qualitatively the evaluation of the role of counter-seepage measures. Discrepancies noted between the recommended calculated structure stability and the operating experience data require that latent additional safety factors of the structure be evaluated. It is necessary to develop new standards for de- signing concrete gravity dams an the basis of their limit atability. V. 0. P. Card 3/3 SOV/!24-58-1-903 Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 1, p 120 (USSR) AUTHORS: Lornize, G.M., Nasberg, V.M TITLE: r_-C,,sid, ration of the Pu;*~ability of the Concrete in Seepage Cal- culations for a Tunnel (dk~t vodopronitsayemosti betona v f il' - tratsionnykh raschetakh tunnelya) PERIODICAL: Tr. Mosk. energ. in-ta, 1956, Nr 19, pp 216-240 ABSTRACT: The authors present a method for the approximate seepage cal- culation of drained and nondrained atmospheric hydraulic tunnels with consideration of the permeability of the tunnel lining under the following premises: The seepage fiow is plane and steady; the relative depth of the tunnel with respt!ct to the free ground-water level exceeds the perimeter of the cross section of the tunnel so much that the surface of seepage may be considered to be approx- imately coincident with a horizontal surface; the soil and the con- crete of the lining are assumed to be uniform and isotropic relative to permeability, and the seepage of the water follows the Darcy law. In finding the calculational relationships for the case when the Card 1/2 tunnel is drained at the bottom, the authors use a superposition in Consideration of the Permeability of the Concrete (cont. ) SOV/1 24-58-1-903 a plane of the flows that are the result of the presence of point sources and sinks, under the condition that the upper and the lower half-planes have different perme- ability coefficients. An analysis of numerical calculations adduced in the paper enables the authors to arrive at the fuilowing conclusions: If the ratio of the F-rme- ability coefficient of the concrete of the tunnel lining divided by the permeability coefficient of the soil exceeds 0. 1, then draining the tunnel is not practicable; if that ratio is less than 0.05, then the tunnel can be drained effectively, in which case the permeability of the lining may be safely disregarded in seepage calcula- tions. Bibliography: 7 references. S. N. Numerov Card 2/2 IDMIZI, G.M., dekt*r takhnichaskikh nauk, professor; NXTUSHIL, A.V., dektor ""JO~~theskikh nauk, professor. Using elactrossmosis in lowering ground water 2evel. Gidr.stret-25 no-3126-31 AP '5b. OGBA 9: 9) (Blectroesmosis) (Water, Underground) S oj~ Cq. L 2 - 21 I - ,1 7 7 r- - 1,,j, ';; T . I I I- L- E U, . LOMIZE, G.M,, doktor tekhn.nauk, prof.: GRIGORYAN, A.A., lnzh. Deformations in loses soils. Gldr.stroi. 26 no.9:27-33 S 157. (MIRA 10:10) (Soil mechanics) ILIASE I BCOK EX?LOITATION SOV/5203 Lomize, Grigoriy Mikhaylovich, and Anatoliy Vladimirovich Netushil ----------- Elektroosmoticheskoye vodoponizheniye (Electro-Oamotic Depression of Water Level (Dewatering]) Moscow, Gosenergoizdat, 1958. 175 P. 2,700 copies printed. Ed.: G. M. Mariupollskiy; Tech. Ed.: A. M. Fridkin. PURPOSE: This book is intended for technical personnel in planning, construction, and scientific research organizations. COVERAGE: The authors describe the results of theoretical and ex- perimental investigations of electro-o:3mosis phencmena in the soil and of electro-osmotic depression of the water level and Its prac- tical application in the USSR and abroad. Acoording to the Fore- word, this is the first attempt to present a generalizatita of the experience gained in this field and to develop practical methods of designing the ansemblies in question. Chs. I and II and Pars. 1 and 2 of Ch. rf were developed and written by Card---I-~ Electro-Osmotic Depression (Cont.) SCYV/5203 G. M. Lomize, Professor, and Ch. III and Pars. 3, 4, and 5 of Ch. IV by A. V. Netushil, Professor. Ch. II is based on the re- search work carried out by th6 Department of Foundations, Earth- works, and Constructions of the Moskovskiy energeticheskiy institut (MEI) (Moscow Power Engineering Institute) under the supervision and with the participation of G. M. Lomize. The following in- vestigations are of special Interest: on electrostabilization of the soil, by Ye. P. Kudryavtsev, Engineer; on the electro-osmotic factor, by R. S. Ziangirov, ingineer; and on the effect of direct current on the filtration properties of clay soils, by A.A. Mukh1n, Candidate of Technical Sciences, and R. S. Ziangirov. Ch. III contains the renultr of theoretical and experiment'al investiga- tinns made at the Deoartrient of Theoretical Principles of Elec- trical Engineering o-.' the NEI under the supervision and with the participation of K. M. Polivanov, Professor, and A. V. Netushil. K. A. Krug, Profp:ssor, Corresponding Member, AS USSR, helped supervise the work, much of which was carried out by N. M. Burdak and A. A. Mukhin, Candidates of Technical Sciences. Ch. IV con- tains a generalization of practical work in the application of 6 Electro-Osmotic Depr,~13,s,-_on (Cont.) SOV/5203 electro-osmotic dewatering In field operations. A. A. Mukhin, N. M. Burdak, Ye. P. Kudryavtsev, R. S. Ziangirov, S. K. Andreyev, I. A. Shekhtman, I. Logov, S. A. Levitan, and o'hers took part in this phase of the work. The MEI Investigations of the effect of direct current on the ao.11 and on the water In it have been con- tinued beyond the publication date, and, according to the Foreword, brought to light new data on the electrical stabilization of the soil, the effect of direct current on filtration and other soil properties, and the poss:Lbility of using the direct current effect on the statics of ground masses. Rather than delay publication of the first reports on this subject, the authors decided to include the developments, corrections, and new information on electro- osmosis and Its applicat4.ons in the next issue of MEI proceedings. The authors thank G. M. liariupollskiy, Candidate of Technical Sciences, for his assistance. There are 62 references: 53 Soviet, 4 English, 3 German, 1 Italian, and I Polish. TABLE OF CONTENTS: Foreword 3 C`P__r-d -_V6 98-5e-6-2/21 AUTHOR: Technical Sciences, Professor TITLE: FiFld of -11-fil.,Lcatior and Schemes of Electro-Os- motir" Level (Obl"st' vozmozhnogo primene- niya J. s~.i, vodoponizheniya) PERIODICALt Stroii.ellstvo, 1958, Nr 6, PP 7-12 (USSR) ABSTRACT-. The r-"- Fcocess can be successfully used to lower the ;-'rourid water in trenches and foundation pits in clay arii --!..%1j--!3andy water-saturuted soils of low dens-ity, 'J.ht~ a%c~*-,.r describes in detail the scheme in which ordinary Gra:.aln.7 we! Is are used as cathodes, and iron rods of diffs7-arill !orr.,, c.riven into the soil are used as anodes (Figure J.) ~ Thit3 rj~,h--3me was elaborated by the Nauchno- is-nledovat,,! :31-,-:.y ~.nQtitnt osnovaniy i podzemnykh sooruzhe-. niy - Sr..`-ont4fit, Regaarch Institute of Foundations and Under- gruund 0cnq4ruct:.on3 -- (B.S. Fedorov, B.A. Rzhanitsyn). The work was done -~-,nder the supervision of the Doctor of Technic- al Sciencuc, A.V. Netushil. There 5 f *-t~-,,..---,:,,, and 10 references, 8 of which are Soviet and 2 Engliah. AVAILABLE: Library ,)f Card 1/1 Hydroloff-USSR 3. Anodes-Applications G1 -rd, 4. Ca"*.-~,)r~~l,.3--.;,.-,o)..-.:-;-:7...~7~:L-- SOV/24-58-'/,-9/36 AUTHOR: Lomize, G. 111. (Mosc.)w) TITLE: _TS_e_Kf~fect of the G:cound Structure on Its Electro-Osmosis (0 vliyanii struktury grunta na elektroosmos v nem) PERIODICAL: Izvestiya Akadantii nauk SSSR OtdeleniyE tekhnicheskikh nauk, 1958, Nr 7, pp 61--69 (USSR5 ABSTRACT! The electro-oamosis of the ground is conFidered by the author in relation to the stream of water h&ving laminar pro- perties. The following factors affect the z:)tir.,a of water (electrolyte); I)a) - soil porosity., m i I., -- the surface of the unit volume of soil s"kel-iton, S 7 (1-1); c) - the characteristic distance L between the eaturated particles with hydraulic radius R m/Jj (E~ 1); J. ) - the shape of the skeleton 'particle,.-,, . 2)a, - density ol.' water P (M, L-3) coefficient of viscosity ji(M, L-1 T-1 9 2 (L T_*l c co6fficien' of kinematic visc-csity -0 - L TJ 3) Velooity Df the interetitia" water (Eq 2, wbere V.- fictitious rata cf the elertro-osmosis). 4) Eloctric power equal to th(, r_~sisuance V,.. (Eq 3, where c volume density of the charge, i.e. sura oi ons, cr '_ as a but related to Card 1/5 3 . S 0 SOV/24-58-?-9/36 The Effect of" the Grouad- Structure or, Its Blectro-Osmosis the unit surfai:.a of Lhe soil skeleton). The eltactro-osmosis J.a described by the '? functions of the exprossion (4), from which the two ~aon-di~ensional values (Eq 5) are defined Reynold's number). Wh--n coefficient of resistance~ -XR, substituting Eq (5) into Eq (4) the formula (6) is obtained, which can te determined experimentally. Also it was found experimentally that the relation between If,.. and V,,,- !, could be e ress6d as: Eq M., where A - a ronstant parameter. When Eq (51 is substitutz-1 into Eq M.. the formula (8) is obtained, while from. Els (2) -9-ad (3) the formula (9) is derived (K, - coefficient of electro-o=sis = fictitious rate of eleotro- osmosis I/,, at th-- tension -,-f the external electri,% field 1 V/cm.)~ PA-LIS7 the formula (9) desnribes the specific property of the electro-osmosis and K r--ipresents thn preparation of the soil., all the par-ticles o.L which are affect-ed by the Card 2/5 SOV/24-58-7-9/36 The Effect of the Ground Stru~tt:.re on Its Electi-c-Osmosis electro-osmositic water flow,, In the case of larger soil particles (sand) the increased dimension of the pores causes changes in the water motion augl the formula (9) must be ad-- justed accordingly, The cuT-eg of the elect'ro-osmosis rate are shown in Fig 1 (e. - fine) b - coaxsel., ',;-- intermediate size of pores, g - linaar ra-i;e. The relation of the surface of the soil ske_~etcn and the hyd-raulic radius f-o the size of the particles and porosity is giver, by Eq (11), whier, when substituted into E (9) ard (10) gives formula (12) tfine particles, and (13'3s(coarse particles), The experimental verification of the above calculation was made by R. S, Ziangireav by metuio ;-,f a -osmCsis master, illus- trated in Figs 2 and (I. - water supply, 2 -- level contTol, 3 - cathode F,~ , -~ a_nGde F--- : 5 - water outlet.). The samples of soi.l_ wo-i- submitt~-_, ior t-be tests incrder -,o de- termine a relatim-Z--~jip c4 ~h~ ele-Itr., -osmosis arid thc- poro.- sity and the ri.. ze of -.*.ie par Les. The samples &r-_ described in the Table in p 64~ walcn -,aver, the actual diameter (2nd column) and upe mear. uianA-~Z- (3:rd -olum:n) and tile 6 :amples of soil (1st colum .). TI.P, desc-r-'.;A-;.on of the Samples is given in the 4th column t'fln'v1oF1a-ia.. oand, screened- river sand, Card 3/5 1 1 SOV/,Z4-58-?-9/36 The Effect of the Ground Structir-a on ire E!Ectro-Osmcsis screened, ocasta.L sanJ , sc rc . aed; laxF;hallit, waLiLed) and the mineral content in the 5th column (rolled grains of qijartz mixed with the spa2- &-.d flint.~ sli-ghl7ly rolled irains of quartz mj_xed with da~rk r_olouz-ed minerals, sharp splinters of quartz3, The resul-.9 cf thla :-xperiments are shcwn in Fig 4; which represents ~he rivLation.ship of the co- efficient Y. (nm s and t h,- , -~ -r n for o,,- - si,_ of g:ai a (mm) various pcro-Aaos i "Ipcinte 1--4- T~61)1-~.Sent n 4B.- 45~O... 37.5 and 34.0 re ape,,-. thscye' 'i.-al cur're). culation of the r.aL b~, porfcrwed i-L re5pect to the zeta-potentia.I a-, in (Eq '.'14))~ Then the ivi-I 'te &1I.Aied as -r-. relation of its rate to'the density of t-he -~urreat fEq 15). Th.e through a crose-sectic-ri of thp, ground c~_ui be lexp~7essed by Eq (16) ( i - current, y -- c,f t;Lc. coil)~ The rate of the ('Ea 1?) was cal:zulated by I,, I~ Zhukov (Ref 1). ThF. _ut,put waz define'_ by him ais Eqs (18) and Card 4/5 SOV/24-58-7-9/36 The Effect of the GrozmC Structure on Its Electro-Osmosis (19). In order to include the structure of the ground in these equations the formula (20) could be applied, The co- efficient of filtration K, can be defined as Eq (21) or (22) and the relation K -7-, car be found from Eq (23). The results of the experimental determination of K in rel- ation to the diameter (d) and porosity (m) of the homogeneous soil are given in Fig 5. There are 5 figures, 1 table and 9 references, of which 8 are Soviet and 1 English, SUBMITTED: June 24, 195?. Card 5/5 10MIZEI G.M., prof.. doktor tekhn.nauk; NABBERG, V.M., kEmd.tean.nauk SeeFage calculations for Iqdraulic tunnels. Izv.VNIIG 58; 162-176 158. (MIRA 13:7) (Boil percolation) (Tunnels) LNIZE, G.A. Consolidating nxcavatinne bjv means of direct currents havirg an influence on static propertioR of clayey Rolls. 16tich.dokl. vya.shkoly; strol. no.1:119-126 159. 041RA 12:10) 1. Rekomendovana kafadroy o9novanly fundajentnv t konstrukt917 Hoskovnkogo onnrgoticbeekogo inRtituta. (Soil stabilization) LOMIZE, G.M. Regularities of deformability of dispersed soils., Nauch.&okl. 4 vyaahko .ly; strol. no.2:121-128 '59. (Kj-M 1-~-.4) 1. Rekomnndovana kafedroy oanovanty, fundamantov i konHtruktniy Hoaknvakogo onergetichaskogo instituta. (Soil machunics) (Plasticity) I I- "I -~~ I LOMIZE I G.M. P -doktor tekhn.nauk, prof. I CP 1~-IRtinw sag defonatione (,.~ locis collB. Gldr. strol. 31 ro.7: I. 39-43. J1 16L (MIRA 14:7) (Loess) LOMIZZ, G.H., doktor tekhn.nauk, prof.; GILIMAII, Ya.D., f.nzh. Electric spark method of compacting soil. Gidr. strai. 32 no.6.*42 A 162a (141RA 15:6) (Soil stabilization) j LOMIU , G.M.; GUTKIN, A.M.; ZHUROV, N.V. Measurement of the conditionaIly instantaneous modulus of elasticity in tenacious sollo, Inzh.-fiz. zhur. 5 no.6:61-66 Je 162. (MIRA 15:12) 1. Energeti-choskiy-inatitut, Moskva. (Elasticity) (Soil research) -LOMIZE, G.M,,- GUTKIN., A.M.; ZHUXOV, N.V. Study of the rheological properties of plastic clays, Ozn,p fund i mekh grun. 5 no.2.1--4 163. (MIRA 16:3) (Clay--Test4ng) LCMnE, ox., prof., daktor taklan. nauk; GILIMAN, Ya.D.p inzhe Compacting soils by electric discharges. Trudy Giproyodkhoza no.22sl55-162 163. (MIRL M8) SM. H. 1 WALM.L.R. .,[transiator]; M0NO8OV,ya.A.[tr&nslAtor]; KOSTY,LWA,V.ye. Xf-ra--54N , HIRDWIOV,G., redaktor; NOGILVSKIT, Yu,A., redaktor; IOVLWA,U.A., tokhnlchaskiy rodaktor [Topics in guided wave propagation through gyromagnatic media. Trans- latod from the Ing3lehl Yoprosy volzxovodnogo rasprostraneniia elektro- magnitnykh voln v girotropnvkh sredakh. Peravod a angliiskogo L.G.Lo- mize, IA.A.Monosova i VJKostylevoL. Moskva, lzd-vo inostrannoi lit-ry, 1955. 189 P. (MLRA 9:3) (REAio waves) (Wave guides) (IlectrowguetLem) 44 P)I) Y-e (7 YOjrS,A:J~.-.MILLJM.S-Y6-. VICIS,K.T.; L(XIZB,L.G.[~wranalator];KIRD(ANOV, Ruben Gayevich, redalctor; KRM(C' ~redaktor; KCRMJV,X.N.. tekhaicheskiy redaktor [Behavior and application of ferrites in the niorowave region. Translated from the Inglishl Svoistv4 ferritoy i ikh primenenie v diapasone SVCH. Perevod a angliiskogo i,.G.Lomize. Moskva, Izd- vo "Sovetakoe .,adio.0 1956. 99 p. (KLRL 9:3) (Yerromagnatim) -4c C M Z' AUTHoR: Lomize, L.G. log-10-11/3'9 TITLE: Anomalous Rotation of the Polarisation Plan," Caused by the Volume Resonance in a Gyro-magnetic Wavegu-de of Finite Length. (Anomallnoye vrashcheniye ploskosti polyarisatsii, obuslovlennoye obleMnym rezonansom v giromagnitnom volr-- ovode konechnoy d1iny PERIODICAL: Radiotekhnika i Elektronika, 1957, Vol-II, No.10, pp. 129? - 1 99 (USSR). ABSTRACT: Some experiments were carried out on a cylindrical wave- guide which was completely filled with a ferrite material. It was found that as a result of strong reflections from the surfaces of the ferrite, a volume resonance was taking place which led to the appearance of a non-linear effect. The non- linearity consists of an anomalous rotation of the folarisation plane, as can be Been from two experimental curves takenl'o-r- two different samples) shown in Fig.l. The curves show the rotation of the polarisation plane as a function of the mag- netising field applied to the ferrites. The above effect could be explained theoretically and calculations were made for a waveguide having a len6th of 1.19 cm, radius of 1 cm and operating frequency of 9 120 Me/s; the ferrite was assumed to have a Cardl/2 permittivity of 10. The calculated curves which are shown in Fig.2 are in good agreement with the experimental data. log-10-11/19 Anomalous Rotation of the Polarisation Plane Caused by the Volume Resonance in a Gyro-magnetic Waveguide of Finite Length. There are 2 figures and 3 Slavic references. SUBMITTED: February 27, 1957. AVAILABIB: Library of Congress. Card 2/2 AUTHORS: ~Jirimanov, R.G., Lo.,mizeL.G. TITLE: Some Titanpte Ferr4_t0G at Ultrahi.-,h r1req enci(-,-0i(-1..o~3rjye j - .-U titanatov~ye ferrit7 na sverldivysokyk?i cliastota:,--'a) PERIODICAL: Radiot,,1z1hni1z-.a iE'lektronilca, 1,)5,3', Vol.I11, Ur 1, P-155 (USSR) ABSTRACT: Some wo:c1c was done tjvard3 iner:m:3ing t1ae permittivity of ferrito.-3 by addin:,, to Vl~:,m, a quartity of CoTiO which has E; = 140 and t 'rr6 = 5 :;-r 10-3 at a of 3.2 cm. Curves of -~t and e1i as a fumctio-a of titanate contents are chown in Fir-.21 re)res,~--I~s 0 the Faraday effect in a cylindrical wave-uide for the ferrites with variDus tit,-alatc- c-)ritents. The na.por c~n- tains 2 figures and 2 Russian references. 0 SLEMITITTED: April 117 1957 AVAIIABLE: Library of' Con-ress Card 1/1 .30V/10)-3-7-5/ ~3 AUTHOR: Lomize, L. G. TITLE: A Gyrotropic Cylindrical Waveguide of Finite Length (Girotropnyy tsilindricheskiy volnovod konechnoy dliny) Radictekhnika i Elekbronika , Nr 7, PP 896-307 (USSR) 1 10/58 ABSTRACT: A cylindrical waveguide containing a section filled -,,.,ith a f-rrite material is considered (see Fig.1). The ferrite is assu,med to be ma,,netized in the longitudinal direction. It is assumed that the waveguides on both sides of the ferrite are semi-infinite and have zae same diameter as the ferrite section. A linearly polarised H 11-viave Dropa- ~,,-,ates along the axis z towards the ferrite section. The problem consists of determining the sl*ft 7 4) , o. the plane of polarisation and the ellipticity, 1 7of the H 11-viave (see Fig.1) which propagates in the 1 ft-hand serii-infinite waveguide. It is necessary to relate ~ and tSQ to frequenzy f the length of the gyrotropic section Card 1/4 3OV/l0*9-3-?-5/23 A Gyrotropic Cylindrical Waveguid3e of Finite Length radius of the waveguide R I the permittivity of the ferrite E and the components of the ferrite tensor ~Ll ~L2 and 1L3 . For the purpose of analysis it is assumed that the losses in the ferrite can be neglected. The solu- tion of the Maxwell equctions for the gyrotropic section can be expressed (Ref.4) by Eqs.(l), vibere J n is a cylin- drical function of the first kind of the n'-h order, r is an arbitrary radius, (p is the azimuth, while the other parameters are defined by the equations on p 89?. The arbitrary constant M of expressions (1) can be determined from the boundary conditions at 'the walls of the waveguide while the constant A n-0 can be evaluated from the boundary conditions at the facial planes of the gyrotropic waveguide. The propagation constant y is given by Eqs.(2). If the electrical radius of the gyrotropic section is large (about 4 times greater than that of the isotropic waveguide), the propagation constants of various waves in the ferrite can be expressed by Eq.(3). The shift in the plane of polari- sati3n and the e114 pticity at the output o~ the Syrotropic Card 2/4 waveguide a:~-e given by Eqs.(6) where the parameters n and 1-73 OVII 09 -3 -7-5/2:; A Gyrotropic Cylindrical Waveguid,~ of Finite Length v are determined by the romaining equations on p 901. Eq3.(6) are employed to plot 0 and tgQ as a function of t for various values of IL2 ; the resulting curves are shown in Figs-3 and 4. 4) as a function of 112 for various values of ~Ll is plotted in Figs-5 while tgO as a function of 112 for various values of Ii, is shown in Figs.6. The families of curves of Figs-5 can be used as nomograms for ui approximate determination of the tensor components of mag- netized ferrites. The basic quantities in this case would be the polarisation planes 4), and 02 for two ferrite samples having different electrical thicknesses; the experi- mentally determined q), and (P2 can be u-sed in conjunction with the curves of Fig-5 to determine curves of q), = const and 4)2 = const in IL, and 112 coordinates. The point of intersection of these curves corresponds to the unknown values .1 I"ard 3/4 ~OV/l' 19-3-7-5/23 A Gyrotropic Cylindrical Wave,,-,uide of Finite Length of ~Ll and 112 . This method was employed to deter;-Ane jil and TL2 for a magnesium-manganese ferrite at a Yjave- length of 3.2 era. The dependence of ~tl and 112 on the magnetizing field H is shown in Fig.?. The paper contains 8 figures and 8 Soviet references. SUBMITTED: February 27, 1957. 1. Waveguldes--P~Vsical properties 2. Ferrites--Magnetic properties 3. Electromagnetic waves--Propagation 4. Mathematics Ca,-,,d 4/4 LCKM, L. G., VYSTAVKIN, A. M. and BMNASBSVSMI G. A. "Rediation of Relativistic Electron Flow at Millimeter Waves, report presented (by Bernashevskly) at the 9th SYmPosium an Millimeter waves, 31 31 Merch - 2 April 1959, Brooklyn Polytech. Inst, Now York. Inst. for Radloeleotriolty wd Electronics, LaS 69913 /60/005/05/001/021 5/109 31 0 0 , E140/E435 AUTHOR: Lomize, L.G. TITLE; Ca lcula ti-o-n-o-T---%-- Cher en!cov Radiator in the '-Ii-.rowave Band ~5 PERIODICAL: Radiotekhnika -4 elektronikia, 1,.)6o,, Vol 5, Nr 5, pp 707-719 (U.5SR) l ABSTRACT: 'of an extended In this article the Cherenkov- radiatiofi beam in wavs-Suidr- sy"5 ems with dieleCtr]C filling 13 considerea. It is shown that wa-veguide Cherenkov radiators are substantially bettf,~r than horn-type devices used experimental!.-/ fRef Id- to 14)~ bas~--d (.in the extraction ~Df energy -In an unbounded dielec,~ric in the direction perpendicular to the beam moiior.. As sbown in th,4 work of other authors fR2f 20114)~ in the millimeter band waveguida d9lay structures ha-e subatantial advantage!5 over resonant sy5tems~ The author first considers the Cherenkov ra,~~iation of a rnre-biinchel el,~!ctron boa.:, in an unbounded diel~!ctric. A quantity Rr is defined aa the radiation resi3Tance and is a function of the radiator parameters anA the velocity and transverse Card 1/3 structare of the electron beam. The case where the beaw C 9 11 S/log/6o/005/05/001/021 E14o/E435 Calculation of a Cherenkov Radiator in the Microwave 1jand uniformly fills the entire channel section is considered, If the bunching remains constant infrease of beam energy above 1 to 2 MaV gives a very slow inc::-ease of' Rr- With sufficient length of waveguide there is a clearly expressed resortant behaviour of R, at 5ynchronism between the current wave and the ele--tromagnetio wave. The resonant frequencies for various wara mcdes differ. An expression is found for the envelope of the frequency characteristic RrO + Rx,zE:s W~ permitting qualitative evaluation of the radiator operation without solution of the dispersion equation. Wi.th increa3e of waveEii'de radius or decrease of length of radiating sectio 11 , the individual resonance curves overlap and a continuous resonance zone occurs. The quantity RrO is directly proportional to f~ Thie is in agreement with the we-l-known fact that Cherenkov radiation power is proportional to frequency. In the presence of a channel in a dielectric the dependence of Rro on F, and f should change substantiaXly, The author .-ecimmi-tids tho~ Card 2/3 following three foums of Chereffliov radiator- ;~q- -3 S/109/0-0/005/05/601/021 E140/E435 Calculation of a Cherenkov Radiator in the !4icrowave Band 1. A selective radinior tuned to some one harnionic contained in tfie be(-.;; C should be taken betw,~en 5 and 10. Resonance should be designed for the E01-wave 2. Broadband radiator, tuned simultaneously to a number of beam harmonies. Th-~, ftindamental re-sonance 4.L-; to-hen for the E02- or E03--WPtvo ~-"th the distance biAween two resonances as closely as jjos.3ible equal tc. tbe beam bunching freqneney or its harmonic, 3. Broadband radiator operating in the continuouz- resonance zone. For the first two cases, tuning is most easilv obtained employing a ferrite-dielectric rriixtur~a instead of a pure dielentric. Tuning is then obtained by variation of the mngnctic teristor of thc ferrite.. Tlv~ work was directed by Berriashevskxy and tht- a-~signvd- current method of' sclving the waveguide. problem employed in the paper was suggested by Vystavkin. There are .11 figures and 20 re:,ferencezi, 10 of which are Soviet, 4 English and 6 Englis)i in Rusiian translation, SUBMITTED: May 11, 1959 Card 3/3 S/109/60/005/06/012/021 E14o/E163 AUTHORS. Anisimoval Yu.V.j Bernashevskiy, G.A., V`_YSMV=T', A.N., an-T- omlze, L.u. TITLE: Millimeter-Band Inve;t`1gatTon Waveguide RadiatOTS Excited by Relativistic Electron "treams --- Q, .- -1 PERIODICAL: Radiotekhnika I elektronika, 1960~ Vol 5. Nr 6, pp 969-980 (USSR) ABSTRACT: In previous theoretical and experimental studies In this field rilativistic beams were used, accelerated and bunched In linear electron accelerators or accelerating resonators, fed by power resonators in the centimeter waveband.,VMagnetic undulators and resonators operating at higher oscillation modes have been used, including dielectric-filled. The radiation power obtained experimentally was as a rule 10 to 100 mW in the longwave portion of the millimeter band but reduced to units or tenths of microwatts at waves of the order of 2 to 3 mm, apparently as a result of insufficiently good bunching Card of the beam. Cherenkov-radiation experiments were 1/5 carried out only for low-voltage beams (of the order of 10 0), The radiation power obtained was a fraction of S/109/60/005/06/012/021 F.140/E163 Millimeter-Band Investigation of Waveguide Radiators Excited by Rej.ativistic Electron Streams a microwatt at a frequency of 24. Ocs, coinciding with the I mching frequency of the beam. In general Cherenkov radiation In the milli-meter region has not been studied experimentally and the theoretical calculations have been carried out for single electrons moving In an unbounded space or an infinitely long 1,raveguide and for an extended electron beam in an unbounded dielectric medium. Such different approaches .o the problem make comparison difficult. In the present work different waveguide radiators are studied from a common point of view and an attempt is made to narrow the existing gap between theoretical and exDerimental results. The present article considers the foilowing three types of waveguide radiators$ smooth waveguide of finite length with rectilinear electron beam, dielectric field waveguide (Cherenkov radiator), Card magnetic undulator. The approach is to consider the 2/5 radiation resistance R as the quantity fully characterising a given radiator. In a smooth waveguide Fq587 E 1109/60/00 5/06/012/021 1'240/B163 Millimeter-Band Investigation of Waveguide Radiator3 Excited by Relativistic Electron Streams the radiation resistance -_beaches appreciable levels and therefore the radiation in such a waveguide may be observed experimentally without difficulty. For a Cherenkov radiator with a long dielectric delay structure it is difficult to realise synchronism simultaneously at several beam harmonies. It i_- therefore useful to employ ferrite delay systems permitting regulat---on of the phase velocities of various waves by magnetic bias of a constant longitudinal magnetic field. The maximum radiation resistance in the Cherenkov radiator at a given frequency occurs for a channel diameter coinciding with the beam diameter and a waveguide diameter calculated from the condition of synchronism for the Eoj-wave~ For the undulator maximum power is radiated at transverse dimensions of the rectangular waveguide equal to the beam width and the sum of the electron oscillation amplitude Card and the beam thickness respectively. The optimum design 3/5 of a smooth waveguide rad' 'Ptor corresponds to a walreguide diameter equal to the electron b.~am diameter (not below ~.Q" - t S/log/6o/oo5/06/012/021 31140/H163 Millimeter-Band Investigation of Waveguide Radiatcrs &Y-cited by Relativistic Electron Streams critical). The length of synchronised radiators is taK(3111 equal to L = 10 am. kt this length the efficiency of synchronised radiators is substantially higher than the efficiency of non-synchronised radiators. The efficiency of the Cherenkov radiator for the present example is substantially greater than the undulator efficienoy. kn experimpntai study of these radiators was carried out using a,linear electron accelerator operating in the 10 cm band with output energy 0.5 to MeV and pulse current 30 to 50 mk, the tested radiator and a set of measuring instruments, The harmonic composition of the electron beam was not studied. experimentally. Therefore the values of R obtained are only relative, They are somewhat low for the following reasons: the shape of the 'bunch a,, the accelerator output may differ substantially from Card rectangular; in calculating R reflect *'on. absorption 415 and conversion losses in various elements ok the channel were neglected; the radlation power of the investigated S/.109/60/005/06/012/021 E140/E163 Millimeter-Band Investigation of Waveguide Radiators Excited by Relativistic 'Electron Streams signal sometimes reached tens of milliwatts compared with a calibration signal of 45 IN. It was assumed that the detector characteristic is quadratic. On the average in the range from 10 to 2 mm a decrease of radiation Power with decrease of wavelength was observed generally constituting approximatel 1 dB per harmonic. There are 11 figures, 1 table and 1K references, of which 15 are Soviet and 1 is English. SUBMITTED: August 20, 1959 Card. 515 83274 s/log/60/005/009/024/026 9140/E455 AUTHORs Lomize, L.G. TITLEs On Transit --and Retardation Radiation in Waveguide Systems PERIODICALs Radiotekhnika i elektronika, 1960, Vol-5, No.9o PP-1546-1549 TEXTs It is shown that if a finite length of modulated electron beam is assumed, a unified treatment of Cherenkov, transit. and retardation radiations may be applied. A plane waveguide system is considered in the assigned-current approximation, after which a rectangular waveguide is examined. With J, ----,b the transit radiation power should be of the same order of magnitude as the retardation power, somewhat exceeding the latter. This was checked experimentally in a rectangular waveguide 3 x 20 mm, with 3 MeV electron beam. One of the wide walls of the waveguide was made of a foil transparent to the electron stream. The waveguide was matched at one end and connected at the other to a measurement circuit reacting to the HIO wave (Ref.11). The experimental results c~,rzfirmed the calculations. Calculations showed tAat, at relativistic velocities of the beam, Card 1/2 83274 S/109/60/005/009/024/026 E140/E455 On Transit and Retardation Radiation in Waveguide Systems radiation in the direction of the beam is substantially more intense than in the perpendicular direction. This is in ac,-ordance with Ref.l. Acknowledgment in made to G.A.Berrshevskiy for directing the work. There are 2 figures and 15 Soviet references, SUBMITTEDs September 26, 1959 Card 2/2 CHEidlETSKIY, A.V., kand. fiz.-mat. nauk, red.; LOIIZE, L.G., inzb., red.; ANDREYENKO, Z.D., red.; VLASOVA, NJ~, tekhn. red. - [Some problems of physical experimental technique in studying gas discharges] Nekotorye voprosy tekhniki fizicheskogo eksperi- menta pri iosledovanii gazovogo razriado; nauchno-tekh.,icheskii sbornik. Moskva, Gosatomizdat. N0-3- 1961. 120 p. (MIRA 15:5) (Electric discharges thrcpgh gases) - 3 0 ((1rd /1.3a/ 111CS) AUTHOR: Lomize, L. G. 20922 S/057/61/031/003/006/019 B125/B202 TITLE: Comparative characteristics of.Cherenkov, and transition, radiation, and bremastrahlung in the range of short radio- waves PERIODICALs Zhurnal tekhnicheskoy fiziki, v. 31, no- 3, 1961, 301-310 TEXT: The author derives the most important equations for the radiatifin resistance of a Cherenkov.radiator - by taking account of the velocity spread - as well as foi- transition radiation and br;emostrahlung. He then intercompares the efficiencies of these 'radiators. Furthermore, the author reports on the results of the experimental study of a grouped electron beam with 3 - 5 Mev. These results in principle confirm the conclusions drawn from the theoretical calculations made by the author. Instruments of the type of.a magnetic undulator were developed for the first time by Mots, Ton, Whitehearst. The first chapter of this paper deals with Cherenkov radiation by taking account of.the velocity spread of electrons in the cluster. In this connection a cylindrical electron Card 1/9 S/057/61/031/003/006/019 Comparative characteristics of... B125/11202 beam with a radius r. passes a channel with the same radius in a dielectric filling a metallic semiconductor with the radius R. The beam is assumed to consist of a periodi*cal a.equen.,e of electron clusters of arbitrary duration and shape. The electron velocities are adsumed to be distributed in each cluster according to a 'it-type law: dN/dv - 0 with-v> vi and v< v2; dN/dv - N/Av with v 24 v 4, (6(s) I-)] U Card 5/9 Comparative characteristics of... 20922 S/057/61/031/003/006/019 B125/B202 then hold with L/X. With L--*cD Eq. (6b) approaches the first Bum in formula (4). In this case a transition radiation is concerned. With square beams (lateral lenith a) 32LI I I . ILI ) ;~,Tfiinl? nPw L